Abstract
The Sr isotope compositions of pelitic granulites and S-type granitic rocks were measured, and a whole rock isochron age from these rocks is given, with a short discussion on its implication for the evolution of the granulite-facies metamorphism and the genesis of the S-type granitic magma in the Main Zone of the Hidaka metamorphic belt. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 751-754 |
| Number of pages | 4 |
| Journal | Journal - Geological Society of Japan |
| Volume | 97 |
| Issue number | 9 |
| DOIs | |
| Publication status | Published - 1991 |
| Externally published | Yes |
All Science Journal Classification (ASJC) codes
- General Environmental Science
- General Engineering
- General Earth and Planetary Sciences
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